Earth’s water may have been inherited from material similar to enstatite chondrite meteorites
Author(s) -
Laurette Piani,
Yves Marrocchi,
Thomas Rigaudier,
Lionel G. Vacher,
Dorian Thomassin,
Bernard Marty
Publication year - 2020
Publication title -
science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 12.556
H-Index - 1186
eISSN - 1095-9203
pISSN - 0036-8075
DOI - 10.1126/science.aba1948
Subject(s) - enstatite , meteorite , chondrite , astrobiology , earth (classical element) , carbonaceous chondrite , mantle (geology) , achondrite , geology , crust , parent body , geochemistry , formation and evolution of the solar system , early earth , mineralogy , physics , astronomy
An unexpected source of Earth's water The abundances of Earth's chemical elements and their isotopic ratios can indicate which materials formed Earth. Enstatite chondrite (EC) meteorites provide a good isotopic match for many elements but are expected to contain no water because they formed in the hot inner Solar System. This would require Earth's water to be from a different source, such as comets. Pianiet al. measured hydrogen contents and deuterium/hydrogen ratios (D/H) in 13 EC meteorites (see the Perspective by Peslier). They found far more hydrogen than is commonly assumed, with D/H close to that of Earth's mantle. Combining these data with cosmochemical models, they show that most of Earth's water could have formed from hydrogen delivered by EC meteorites.Science , this issue p.1110 ; see also p.1058
Accelerating Research
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom
Address
John Eccles HouseRobert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom